Lipotyphla
Lineage (NCBI):
root
» Eukaryota
» Opisthokonta
» Metazoa
» Eumetazoa
» Bilateria
» Coelomata
» Deuterostomia
» Chordata
» Craniata <chordata>
» Vertebrata <Metazoa>
» Gnathostomata <vertebrate>
» Euteleostomi
» Sarcopterygii
» Tetrapoda
» Amniota
» Mammalia
» Theria <Mammalia>
» Eutheria
» Laurasiatheria
» Insectivora
node name Lipotyphla Look for this name in NCBI Wikipedia Animal Diversity Web | ||
recommended citations http://palaeo-electronica.org/content/fc-1 Benton et al. 2015 |
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node minimum age 61.6 Ma With records from the Torrejonian, the minimum estimate of Adunator can be tied to the top of the Danian at 61.6 Ma ± 0.0 Myr (Gradstein et al., 2012, p. 400; Woodburne, 2004). | ||
node maximum age 164.6 Ma The soft maximum date is based on the divergence of Eutheria from other mammals in the late Jurassic, represented by Juramaia (Luo et al., 2011). This taxon is represented in the Daxigou site of the Tiaojishan Formation, Liaoning Province, Northeastern China, and has been constrained by radiometric dates to derive from deposits of just over 160 Ma in age (Luo et al., 2011). The equivalent marine stage is the Oxfordian (Gradstein et al., 2012), with a lower boundary of 163.5 Ma ± 1.1 Myr, and thus 164.6 Ma is a soft maximum. | ||
primary fossil used to date this node | ||
USNM 9640 | ||
phylogenetic justification
Adunator is a member of Erinaceomorpha, according to phylogenetic analyses by Novacek et al. (1985) and Smith et al. (2002), and so is a nested within crown Lipotyphla. |
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phylogenetic reference(s)
Novacek, M.J. 1985. On the classification of early Tertiary Erinaceomorpha (Insectivora, Mammalia). American Museum Novitates, 2813:1-22.
Smith, T., Bloch, J.I., Strait, S.G., and Gingerich, P.D. 2002. New species of Macrocranion (Mammalia, Lipotyphla) from the earliest Eocene of North America ad its biogeographic relationships. Contributions from the Museum of Paleontology, The University of Michigan, 30:373–384.
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tree image (click image for full size) | ||
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